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Primordial soup, also known as prebiotic soup, is the hypothetical set of conditions present on the Earth around 3.7 to 4.0 billion years ago. It is an aspect of the heterotrophic theory (also known as the Oparin–Haldane hypothesis) concerning the origin of life, first proposed by Alexander Oparin in 1924, and J. B. S. Haldane in 1929.[1][2]
As formulated by Oparin, in the primitive Earth's surface layers, carbon, hydrogen, water vapour, and ammonia reacted to form the first organic compounds. The concept of a primordial soup gained credence in 1953 when the "Miller–Urey experiment" used a highly reduced mixture of gases—methane, ammonia and hydrogen—to form basic organic monomers, such as amino acids.[3]
- ^ Oparin, Alexander. "The Origin of Life" (PDF). Archived (PDF) from the original on 2018-08-22. Retrieved 2018-10-24.
- ^ Haldane, John B. S. "The Origin of Life" (PDF). Archived (PDF) from the original on 2003-09-27. Retrieved 2018-10-24.
- ^ Miller, Stanley L. (1953). "A Production of Amino Acids Under Possible Primitive Earth Conditions". Science. 117 (3046): 528–9. Bibcode:1953Sci...117..528M. doi:10.1126/science.117.3046.528. PMID 13056598. S2CID 38897285.